Geomorphic Analysis Tectonics Using by Nair Aravind (5 results)

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  • Language: English

    Published by LAP LAMBERT Academic Publishing, 2017

    6202052279 / 9786202052276

    • Softcover

    Seller: Revaluation Books, Exeter, United KingdomRevaluation Books

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    Paperback. Condition: Brand New. 60 pages. 8.66x5.91x0.14 inches. In Stock.

  • Language: English

    Published by LAP LAMBERT Academic Publishing Sep 2017, 2017

    6202052279 / 9786202052276

    • Softcover
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    Seller: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, GermanyBuchWeltWeit Ludwig Meier e.K.

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    Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evidence of neotectonic activity, active tectonics, and the occurrence of historical earthquakes. Its frontal deformation zone is characterized, in some segments, by intermountain longitudinal valleys (duns). Such frontal segments of the Himalaya are marked by the occurrence of multiple mountain fronts.(Kothyari, G., 2010; Lee, C. S L, 2010). The main objective is to carry out topographic analysis using DEM data and calculation of geomorphic indices to decipher tectonic deformation, to prepare a geomorphic map of the study area and analysis of surface processes using remote sensing data, Mapping of channel planform parameters such as longitudinal profile, hypsometry, stream gradient index and analysis of river processes in response to tectonic deformation and finally to integrate all the data to model geomorphic response of the Markanda River basin to tectonic deformation. 60 pp. Englisch.…

  • Language: English

    Published by LAP LAMBERT Academic Publishing, 2017

    6202052279 / 9786202052276

    • Softcover
    • Print on Demand

    Seller: AHA-BUCH GmbH, Einbeck, GermanyAHA-BUCH GmbH

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    Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evidence of neotectonic activity, active tectonics, and the occurrence of historical earthquakes. Its frontal deformation zone is characterized, in some segments, by intermountain longitudinal valleys (duns). Such frontal segments of the Himalaya are marked by the occurrence of multiple mountain fronts.(Kothyari, G., 2010; Lee, C. S L, 2010). The main objective is to carry out topographic analysis using DEM data and calculation of geomorphic indices to decipher tectonic deformation, to prepare a geomorphic map of the study area and analysis of surface processes using remote sensing data, Mapping of channel planform parameters such as longitudinal profile, hypsometry, stream gradient index and analysis of river processes in response to tectonic deformation and finally to integrate all the data to model geomorphic response of the Markanda River basin to tectonic deformation.…

  • Language: English

    Published by LAP LAMBERT Academic Publishing, 2017

    6202052279 / 9786202052276

    • Softcover
    • Print on Demand

    Seller: moluna, Greven, Germanymoluna

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    Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Nair Aravind S.Completed Graduation in 2008 from Uni. of Kerala in Geology,Completed PG in 2010 from National College, Bharathidasam Uni. Trichy in Applied Geology.Completed a Diploma in GeoInformatics in 2010 from Centre for Envirnm.…

  • Language: English

    Published by LAP LAMBERT Academic Publishing Sep 2017, 2017

    6202052279 / 9786202052276

    • Softcover
    • Print on Demand

    Seller: buchversandmimpf2000, Emtmannsberg, BAYE, Germanybuchversandmimpf2000

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    Taschenbuch. Condition: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evidence of neotectonic activity, active tectonics, and the occurrence of historical earthquakes. Its frontal deformation zone is characterized, in some segments, by intermountain longitudinal valleys (duns). Such frontal segments of the Himalaya are marked by the occurrence of multiple mountain fronts.(Kothyari, G., 2010; Lee, C. S L, 2010). The main objective is to carry out topographic analysis using DEM data and calculation of geomorphic indices to decipher tectonic deformation, to prepare a geomorphic map of the study area and analysis of surface processes using remote sensing data, Mapping of channel planform parameters such as longitudinal profile, hypsometry, stream gradient index and analysis of river processes in response to tectonic deformation and finally to integrate all the data to model geomorphic response of the Markanda River basin to tectonic deformation.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 60 pp. Englisch.…